Abstract
The heat flux across the interface between a dry snow layer, a slush layer and an ice plate and pavement surface, i.e., pavement heat flux, may be formulized in terms of the thermal contact resistance, Rc. These three kinds of Rc were evaluated from the thermal energy equation using data obtained from heat transfer experiments.
It was found that (1) Rc of the dry snow-pavement exponentially decreases as the snow density increases, (2) Rc of the slush-pavement is constant for the mass ice content, Θi, less than 0.6, but exponentially increases with Θi for Θi≧0.6, (3) Rc exponentially increases with the volumetric air content, regardless of the snow/ice situation.